plate tectonics
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The movement of continents on Earth's surface is known as plate tectonics. This theory explains how the Earth's lithosphere is divided into several large plates that are in constant motion, which can lead to phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
The process by which continents move slowly across the Earth's surface is called plate tectonics. This movement is driven by the continuous shifting of large geological plates that make up the Earth's outer shell. The movement of these plates can result in phenomena like earthquakes, volcanic eruptions, and the formation of mountain ranges.
The idea that continents move slowly across Earth's surface is called plate tectonics. This theory explains how the Earth's lithosphere is divided into plates that move and interact with each other, leading to processes such as earthquakes, volcanic activity, and the formation of mountain ranges.
The process in which continents move slowly across Earth's surface is called plate tectonics. It involves the movement of large plates of the Earth's lithosphere over the semi-fluid asthenosphere beneath them. This movement is driven by heat from within the Earth, causing the plates to separate, collide, or slide past each other.
The hypothesis is called continental drift. It suggests that the Earth's continents were once part of a single supercontinent called Pangaea and have since moved slowly over time to their current positions. This movement is driven by the process of plate tectonics.
The theory that states that the continents move over the surface of the Earth is called plate tectonics. It explains how the Earth's lithosphere is divided into several plates that float on the semi-fluid asthenosphere beneath them, causing the continents to move and interact with each other. These movements are responsible for various geological phenomena like earthquakes, volcanoes, and mountain formation.